KEYWORDS: Sensors, Remote sensing, Signal to noise ratio, Atmospheric corrections, Remote sensing, Absorption, Luminescence, Near infrared, Aerosols, Short wave infrared radiation, MODIS
Selection of central wavelengths, bandwidths and the number of spectral bands of any sensor to be flown on a remote sensing satellite is important to ensure discriminability of targets and adequate signal-to-noise ratio for the retrieval of parameters. In recent years, a large number of spectral measurements over a wide variety of water types in the Arabian Sea and the Bay of Bengal have been carried out through various ship cruises. It was felt pertinent to use this precious data set to arrive at meaningful selection of spectral bands and their bandwidths of the ocean colour sensor to be flown on the forthcoming Oceansat-3 of ISRO. According to IOOCG reports and studies by Lee and Carder (2002) it is better for a sensor to have ~15 bands in the 400-800 nm range for adequate derivation of major properties (phytoplankton biomass, colored dissolved organic matter, suspended sediments, and bottom properties) in both oceanic and coastal environments from observation of water color.
In this study, ~417 hyper-spectral remote-sensing reflectance spectra (spectral range varies from ~380-800 nm) covering different water types like open, coastal, mid coastal and near coastal waters have been used to identify the suitable spectral bands for OCM-3. Central wavelengths were identified based on the results obtained from hyper-spectral underwater radiometer measurements of Rrs, HPLC pigments and spectrometer analyzed absorption spectra for all the above water types. Derivative analysis has been carried out from 1st to 5th order to identify the inflection and null points for better discrimination / identification of spectral peaks from the in situ Rrs spectra. The results showed that open ocean and coastal ocean waters has spectra peaks mostly in the blue, green region; turbid coastal waters has maximum spectral peaks in the red region. Apart from this, the spectral peaks were identified in the red region for the chlorophyll fluorescence in the open ocean and coastal waters. Based on these results 13 spectral bands were proposed in the VNIR region for the upcoming OCM-3 sensor. In order to obtain water leaving radiances from the measurements at spacecraft platform, it is necessary to do atmospheric correction we need to have spectral bands in the NIR and above regions. Hence, a set of bands 3 bands in the NIR and SWIR region were proposed for OCM-3 to address the atmospheric correction related issues.
This paper investigates the estimation of modulation transfer function (MTF) and point spread function (PSF) using onorbit
data of the first dedicated cartographic mission of ISRO, namely, IRS-Cartosat-1. The Cartosat-1 was launched in
May 2005 with a motivation to realize in-track stereo-pair imagery at a ground sampling distance of 2.5 m with one of
its two cameras, AFT, kept to view a ground scene at -5o and the other, FORE, at +26o with respect to nadir. As with
any high-resolution satellite imagery, several factors viz., stray light, optics aberrations, defocusing, satellite motion,
atmospheric transmittance etc. can have a strong impact on the observed spatial quality of the Cartosat-1 imagery. These
factors are cumulatively accounted by PSF or by the MTF in the spatial frequency domain. The MTF is, thus, of
fundamental importance since it provides assessment of spatial response of the overall imaging performance of the
system. In this paper, estimation of the PSF and MTF was carried out by capturing imagery over airport runway strip as
well as artificial targets laid at two different locations within India. The method adapted here uses a sharp edge from two
adjacent uniform dark and bright fields or targets. A super-resolved edge of sub-pixel resolution was constructed from
the image edge slanted to satellite path to meet the basic requirement that the target width is much smaller than the
spatial resolution width. From the preliminary results, the MTF for the FORE is found to be approximately lesser by
about 2% with respect to AFT; this difference may be attributed to relatively a longer traverse of ground signal through
the atmospheric column in the case of FORE camera.
Microwave remote sensing is one of the most promising tools for soil moisture estimation owing to its high sensitivity to dielectric properties of the target. Many ground-based scatterometer experiments were carried out for exploring this potential. After the launch of ERS-1, expectation was generated to operationally retrieve large area soil moisture information. However, along with its strong sensitivity to soil moisture, SAR is also sensitive to other parameters like surface roughness, crop cover and soil texture. Single channel SAR was found to be inadequate to resolve the effects of these parameters. Low and high incidence angle RADARSAT-1 SAR was exploited for resolving these effects and incorporating the effects of surface roughness and crop cover in the soil moisture retrieval models. Since the moisture and roughness should remain unchanged between low and high angle SAR acquisition, the gap period between the two acquisitions should be minimum. However, for RADARSAT-1 the gap is typically of the order of 3 days. To overcome this difficulty, simultaneously acquired ENVISAT-1 ASAR HH/VV and VV/VH data was studied for operational soil moisture estimation. Cross-polarised SAR data has been exploited for its sensitivity to vegetation for crop-covered fields where as co-pol ratio has been used to incorporate surface roughness for the case of bare soil. Although there has not been any multi-frequency SAR system onboard a satellite platform, efforts have also been made to understand soil moisture sensitivity and penetration capability at different frequencies using SIR-C/X-SAR and multi-parametric Airborne SAR data. This paper describes multi-incidence angle, multi-polarised and multi-frequency SAR approaches for soil moisture retrieval over large agricultural area.
In this paper an attempt to model wheat yield is made by exploiting characteristic interaction of cross-polarised SAR with wheat crop. SAR backscatter from a crop field is affected by the density, structure, volume and the moisture content of various components of plant (viz. head, stem, leaf) alongwith soil moisture. Hence, to effectively handle the influence of each of these components of the plant on SAR backscatter, a plant parameter, termed as Interaction Factor (IF) is conceptualised by combining volume, moisture, height for each of the component and density of plant. For this purpose, detailed experiment over farmers' fields was carried out in synchrony with SAR acquisition involving in-depth measurements on volume, moisture content and height of various components of wheat plant, number of grains, plant density and soil moisture. Stepwise regression analysis revealed that IFHead significantly affects the shallow incidence angle, cross-polarised C-band SAR backscatter. IFHead is also highly correlated to the number of grains. This is attributed to the fact that parameters of the wheat head from which IFHead is calculated, namely moisture, volume and height, determine eventual number of grains. The study offers an approach for estimating wheat yield by retrieving number of grains from shallow incidence angle cross-polarised SAR data.
Indian Earth Observation (EO) Programme, since its inception has been applications driven and national
development has been its main motivation. In order to meet the observational requirements of many societal
benefit areas, a series of EO systems have been launched in both polar and geo synchronous orbits. Starting
from Bhaskara, the first experimental EO satellite in 1979 to Cartosat-1 successfully launched in May 2005, a
large number of sensors operating in optical and microwave spectral regions, providing data at resolutions
ranging from 1 km to a meter have been built and flown. Data reception and processing facilities have been
established not only in the country but also at various international ground stations. Remotely sensed data and
its derived information have become an integral component of the National Natural Resources Management
System (NNRMS), a unique concept evolved and established in the country. The paper discusses the
evolution of IRS satellite systems, application programmes in different societal benefit areas and the road
ahead. How it complements and supplements the international efforts in the context of Global Earth
Observation System of Systems has also been indicated.
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